High resolution palynological record off the Iberian margin: direct land-sea correlation for the Last Interglacial complex

Goñi, Marı́a Fernanda Sánchez; Eynaud, Frédérique; Turon, Jean‐Louis; Shackleton, Nicholas J

doi:10.1016/s0012-821x(99)00141-7

Cited by 382 publications

(270 citation statements)

References 37 publications

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“…It lasted for almost 20,000 years (de Beaulieu and Reille, 1992a;Kukla et al, 1997;Kukla, 2000). A close parallel between the concentration of nonarboreal pollen at this site and cold-water foraminifera Neogloboquadrina pachyderma sinistral in deep-sea core V29-191 (Kukla et al, 1997), as well as the pollen record of core MD 952042 (Sánchez-Goñi et al, 1999), indicates that the Eemian Zone at La Grande Pile correlates with the main part of MIS 5e and most of MIS 5d. The boreal forest was abruptly replaced by open vegetation in the silty zone, Melisey I.…”

Section: Pollen Records In Lake Sedimentsmentioning

confidence: 80%

“…However, although they do belong to the same warm episode that peaked during the last interglacial, the upper and lower boundaries may be of different ages Turner, 2000Turner, , 2002a. It now appears that the Eemian pollen zones in France and off Portugal may correspond to an interval considerably longer than that in the Netherlands and Germany, where the Eemian deposits were originally described (Sánchez-Goñi et al, 1999;Kukla, 2000;McManus et al, 2002;Shackleton et al, 2002).…”

Section: Eemian and The Last Interglacialmentioning

confidence: 92%

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Last Interglacial Climates

Kukla¹,

et al. 2002

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The last interglacial, commonly understood as an interval with climate as warm or warmer than today, is represented by marine isotope stage (MIS) 5e, which is a proxy record of low global ice volume and high sea level. It is arbitrarily dated to begin at approximately 130,000 yr B.P. and end at 116,000 yr B.P. with the onset of the early glacial unit MIS 5d. The age of the stage is determined by correlation to uranium-thorium dates of raised coral reefs. The most detailed proxy record of interglacial climate is found in the Vostok ice core where the temperature reached current levels 132,000 yr ago and continued rising for another two millennia. Approximately 127,000 yr ago the Eemian mixed forests were established in Europe. They developed through a characteristic succession of tree species, probably surviving well into the early glacial stage in southern parts of Europe.

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Section: Pollen Records In Lake Sedimentsmentioning

confidence: 80%

Section: Eemian and The Last Interglacialmentioning

confidence: 92%

Last Interglacial Climates

Kukla¹,

et al. 2002

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“…These sec ond ary peaks in ma rine iso tope stages are named with ad di tional num bers or let ters (see Martinson et al, 1987;Railsback et al, 2015). Hence, lo cat ing these turn ing points on iso tope curves al lows cal cu lat ing du ra tion of the inter gla cial on the con ti nent (see Sánchez GoÔi et al, 1999).…”

Section: Discussionmentioning

confidence: 99%

“…Cer tainly, no re li able con clusions should be drawn about smaller intra-inter gla cial and glacial os cil la tions, and the ma rine-de rived pol len spec tra can not be the main base of con clu sions on sub tle de coup ling trends be tween oce anic and land con di tions. The rea sons of these are mul ti di men sional (see S«nchez GoÔi et al, 1999Oliveira et al, 2016Oliveira et al, , 2017. One is a long dis tance of a deep-sea core from the con ti nent (Oliveira et al, 2016(Oliveira et al, , 2017S«nchez GoÔi et al, 2016), which makes pol len that is best-adapted to long trans port to be the main com po nent of the spec trum.…”

Section: Introductionmentioning

confidence: 99%

Terrestrial versus marine archives: biostratigraphical correlation of the Middle Pleistocene lacustrine records from central Europe and their equivalents in the deep-sea cores from the Portuguese margin

Bińka

Marks

2018

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The palaeolake from Ossówka, east ern Po land, is an un usual ex am ple of ba sin, in which sed i men ta tion lasted from the begin ning of the Holsteinian through sev eral cli ma tic os cil la tions un til the Early Saalian, i.e. over a pe riod of ~70,000 years. This pro vides us with the op por tu nity of cor re lat ing the dy nam i cally chang ing events on land with their po ten tial equiv a lents in the ma rine pro files. Alkenone-based tem per a ture re con struc tions us ing U 37 k ¢ are an un usual tool in this re spect. Nev er theless, as a re sult, we suc cess fully re late this pol len se quence to the chang ing SST (sea sur face tem per a ture) val ues in the colder phases of MIS 11. The bi par tite Ferdinandovian Inter gla cial was pre vi ously cor re lated with the up per part of the Cromerian com plex (MIS 13 and MIS 15). Hav ing at our dis posal lim its in the SST alkenone-based re cord, we clearly iden tify the strati graphic po si tion of the sec ond warm phase of MIS 15 and a small frag ment of MIS 14. In our opin ion, the Rhume Inter gla cial, iden ti fied in Ger many, should be lo cated within MIS 13. Us ing the avail able or bit ally tuned chro nol ogy, we also give a sub stan tial in put to es ti mate du ra tion of these ter res trial interglacials, in di cat ing the start ing and end ing points of their equiv a lents in the alkenone re cords.

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“…1 et 2 ;Sánchez Goñi et al, 1999, 2016Tzedakis et al, 2004 ;Chabaud et al, 2014 ;Oliveira et al, 2016 ; données inédites). Le pollen de ce site provient de la végétation du sud-ouest de la péninsule Ibérique, dominée par la forêt méditerranéenne.…”

Section: -La Diversité Des Interglaciaires Des Derniers 425 000 Ans Dunclassified

L’étude du pollen des séquences sédimentaires marines pour la compréhension du climat : l’exemple des périodes chaudes passées

Desprat¹,

Oliveira²,

Naughton³

et al. 2017

quaternaire

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High resolution palynological record off the Iberian margin: direct land-sea correlation for the Last Interglacial complex

Cited by 382 publications

References 37 publications

Last Interglacial Climates

Last Interglacial Climates

Terrestrial versus marine archives: biostratigraphical correlation of the Middle Pleistocene lacustrine records from central Europe and their equivalents in the deep-sea cores from the Portuguese margin

L’étude du pollen des séquences sédimentaires marines pour la compréhension du climat : l’exemple des périodes chaudes passées

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